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- W2099870741 abstract "indicated that the halite dissolution is the source of Cl - and Na + . Weathering silica is the source of SiO2. Results of thermodynamic speciation showed that the groundwater is generally in an equilibrium condition with calcite and quartz. Groundwater is undersaturated with respect to anhydrite, dolomite, gypsum, halite and palygorskite. The mean PCO2 is 1.34 x 10 -3 atm., which suggested a deep closed environment. The geochemical evolution of the groundwater demonstrates that the dedolomitization is a major geochemical process affecting the chemistry of the aquifer. The analysis of the pumping test data indicated that the aquifer is acting as semi-confined with an average transmissivity of 212 m 2 /d, and average hydraulic conductivity (K) of 2 m/d. The aquifer is underlain by a continuous aquitard layer of basal clay and chert that separates the Kuwait Group aquifer from the underlying Dammam limestone aquifer." @default.
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- W2099870741 date "2007-01-01" @default.
- W2099870741 modified "2023-09-27" @default.
- W2099870741 title "GEOLOGICAL, GEOCHEMICAL AND HYDROGEOLOGICAL INVESTIGATION OF MIOCENE-PLEISTOCENE AQUIFER, KUWAIT" @default.
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